Spinels and oxygen fugacity in olivine-phyric and lherzolitic shergottites
نویسندگان
چکیده
منابع مشابه
Estimates of Oxygen Fugacity in the Basaltic Shergottites from Electron Microprobe Oxygen Analysis
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Rb-Sr AND Sm-Nd STUDIES OF OLIVINE-PHYRIC SHERGOTTITES RBT 04262 AND LAR 06319: ISOTOPIC EVIDENCE FOR RELATIONSHIP TO ENRICHED BASALTIC SHERGOTTITES
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Introduction: Recently, a lot of basaltic shergottites have been found from the desert areas in northern Africa and Middle East Asia. Most of them contain large olivine grains that are not present in the previously known basaltic shergottites (except for EETA79001). These olivine grains are mostly Mg-rich, but they show different mineralogical features in each meteorite. Dar al Gani 476 and its...
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Introduction: Lherzolitic shergottites show similar mineralogy and ages [e.g., 1,2], and are widely believed to have originated from the geochemically-intermediate reservoir having distinct trace element and isotopic compositions [e.g., 3,4]. RBT04262 and NWA4468 are recently discovered new shergottites that contain py-roxene oikocrysts enclosing olivine and chromite, and petrographically simil...
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ژورنال
عنوان ژورنال: Meteoritics & Planetary Science
سال: 2003
ISSN: 1086-9379,1945-5100
DOI: 10.1111/j.1945-5100.2003.tb00014.x